文章摘要
张向飞,周维博,云 涛,刘小学,董起广.渭北旱塬区地下水动态研究Journal of Water Resources and Water Engineering[J].,2012,23(1):89-93
渭北旱塬区地下水动态研究
Dynamic research on groundwater in Weibei upland
Received:October 20, 2011  Revised:October 28, 2011
DOI:
中文关键词: 地下水动态  次降雨  ARIMA模型  渭北旱塬区
英文关键词: groundwater dynamics  precipitation  auto regressive integrated moving average model (ARIMA)  Weibei upland
基金项目:陕西省水利厅科技项目
Author NameAffiliation
ZHANG Xiangfei Chang''an University, Xi''an 710054, China 
ZHOU Weibo Chang''an University, Xi''an 710054, China 
YUN Tao Chang''an University, Xi''an 710054, China 
LIU Xiaoxue Shaanxi Bureau of Groundwater Management Monitoring, Xi''an 710002, China 
DONG Qiguang Chang''an University, Xi''an 710054, China 
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中文摘要:
      渭北旱塬区地表水资源短缺,地下水成为城市和农村的重要供水水源,为了掌握该区地下水动态变化特征,本文以渭北旱塬区2000-2009年间水文气象和地下水浅层监测井实测资料为依据,根据地下水补给排泄条件及自然、人为影响因素之间的关系,将研究区地下水动态成因分为灌溉-开采、渗入-蒸发、渗入-开采和径流-开采4种类型,对各类型地下水变化特征进行分析,并运用差分自回归移动平均(ARIMA)模型对地下水位埋深进行模拟预测。结果表明:拟合程度较高,预测效果较好。
英文摘要:
      The surface water resource in Weibei upland is scarce and the groundwater is the main water supply source for city and rural area. In order to analyze the groundwater variation characteristics, based on the shallow observation hydrometeorology data of Weibei Upland from 2000 to 2009, the variation factors were defined as four types (irrigation-exploitation, infiltration-evaporation, infiltration-exploitation & runoff and runoff-exploitation) according to the relationship between the recharge-discharge condition with natural and human activity influencing factors. The groundwater variation characteristics of each type were analyzed and the groundwater depth was simulated and predicted by autoregressive integrated moving average model (ARIMA). The results showed that the model meet the actual data very well.
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